Ocean boundary current systems are key components of the climate system, are home to
highly productive ecosystems, and have numerous societal impacts. Establishment of a …

The timing of the annual phytoplankton spring bloom is likely to be altered in response to
climate change. Quantifying that response has, however, been limited by the typically coarse …

The ocean is currently a significant net sink for anthropogenically remobilised CO 2, taking
up around 24% of global emissions. Numerical models predict a diversity of responses of …

A 3‐D high‐resolution coupled hydrodynamic‐biogeochemical model of the western
Mediterranean was used to study phytoplankton dynamics and organic carbon export in …

The large-scale distribution of thaliaceans in relation to environmental variables was
investigated over 4500 km in the transition region of the North Pacific (36° N–43.6° N, 141.5° …

Phytoplankton bloom phenology studies are fundamental for the understanding of marine
ecosystems. Mismatches between fish spawning and plankton peak biomass will become …

Carbon export out of the surface ocean via the biological pump is a critical sink for
atmospheric carbon dioxide. This process transports organic carbon to the deep ocean …

Multiyear estimates of organic matter (OM) export based primarily on oxygen and dissolved
inorganic carbon surface layer budgets applied basin‐wide for the Pacific, Atlantic, and S …

Abstract The subpolar North Atlantic plays an outsized role in the atmosphere‐to‐ocean
carbon sink. The central Irminger Sea is home to well‐documented deep winter convection …

The oceanic absorption of anthropogenic carbon dioxide (CO2) is expected to continue in
the following centuries, but the processes driving these changes remain uncertain. We …